ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ...
The ApRES (Brennan et al., 2014; Nicholls et al., 2015) was deployed from January to December in 2016 on the RBIS about 90 km from the ice shelf front and 5 km seaward from the grounded ice on the fast-flowing portion of the West Ragnhild glacier, which is the third largest outlet glacier along the...
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Online Access: | https://dx.doi.org/10.1594/pangaea.964065 https://doi.pangaea.de/10.1594/PANGAEA.964065 |
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ftdatacite:10.1594/pangaea.964065 2024-03-31T07:52:29+00:00 ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ... Sun, Sainan Pattyn, Frank 2024 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.964065 https://doi.pangaea.de/10.1594/PANGAEA.964065 en eng PANGAEA https://dx.doi.org/10.1029/2019gl083881 https://dx.doi.org/10.1049/iet-rsn.2013.0053 https://dx.doi.org/10.1002/2014jf003246 https://dx.doi.org/10.3189/2015jog15j073 https://dx.doi.org/10.1126/science.1235798 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 ApRES Ice shelf NECKLACE DATE/TIME netCDF file netCDF file File Size Multiple investigations dataset Dataset 2024 ftdatacite https://doi.org/10.1594/pangaea.96406510.1029/2019gl08388110.1049/iet-rsn.2013.005310.1002/2014jf00324610.3189/2015jog15j07310.1126/science.1235798 2024-03-04T12:41:01Z The ApRES (Brennan et al., 2014; Nicholls et al., 2015) was deployed from January to December in 2016 on the RBIS about 90 km from the ice shelf front and 5 km seaward from the grounded ice on the fast-flowing portion of the West Ragnhild glacier, which is the third largest outlet glacier along the Dronning Maud Land Coast (Callens et al., 2014). The ice thickness at the site was ∼300 m in the trough of a channel (Drews, 2015) but increases up to 600 m in the grounding zone upstream, and ice flow velocities in this region range between 250 and 300 m/a (Rignot et al., 2013). By transmitting an electromagnetic signal and receiving the echo, the radar system can detect the ice base (ice-ocean interface) as well as relatively weak internal reflecting layers that are due to changes in ice permittivity. Between two consecutive measurements, the relative vertical motion of internal layers and the base can therefore be tracked. The displacements of the internal layers determine how the thickness of the column ... Dataset Dronning Maud Land Ice Shelf DataCite Metadata Store (German National Library of Science and Technology) Dronning Maud Land Roi Baudouin ENVELOPE(24.461,24.461,-70.438,-70.438) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
ApRES Ice shelf NECKLACE DATE/TIME netCDF file netCDF file File Size Multiple investigations |
spellingShingle |
ApRES Ice shelf NECKLACE DATE/TIME netCDF file netCDF file File Size Multiple investigations Sun, Sainan Pattyn, Frank ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ... |
topic_facet |
ApRES Ice shelf NECKLACE DATE/TIME netCDF file netCDF file File Size Multiple investigations |
description |
The ApRES (Brennan et al., 2014; Nicholls et al., 2015) was deployed from January to December in 2016 on the RBIS about 90 km from the ice shelf front and 5 km seaward from the grounded ice on the fast-flowing portion of the West Ragnhild glacier, which is the third largest outlet glacier along the Dronning Maud Land Coast (Callens et al., 2014). The ice thickness at the site was ∼300 m in the trough of a channel (Drews, 2015) but increases up to 600 m in the grounding zone upstream, and ice flow velocities in this region range between 250 and 300 m/a (Rignot et al., 2013). By transmitting an electromagnetic signal and receiving the echo, the radar system can detect the ice base (ice-ocean interface) as well as relatively weak internal reflecting layers that are due to changes in ice permittivity. Between two consecutive measurements, the relative vertical motion of internal layers and the base can therefore be tracked. The displacements of the internal layers determine how the thickness of the column ... |
format |
Dataset |
author |
Sun, Sainan Pattyn, Frank |
author_facet |
Sun, Sainan Pattyn, Frank |
author_sort |
Sun, Sainan |
title |
ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ... |
title_short |
ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ... |
title_full |
ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ... |
title_fullStr |
ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ... |
title_full_unstemmed |
ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ... |
title_sort |
apres time series from roi baudouin ice shelf, 2016/02-2017/01 ... |
publisher |
PANGAEA |
publishDate |
2024 |
url |
https://dx.doi.org/10.1594/pangaea.964065 https://doi.pangaea.de/10.1594/PANGAEA.964065 |
long_lat |
ENVELOPE(24.461,24.461,-70.438,-70.438) |
geographic |
Dronning Maud Land Roi Baudouin |
geographic_facet |
Dronning Maud Land Roi Baudouin |
genre |
Dronning Maud Land Ice Shelf |
genre_facet |
Dronning Maud Land Ice Shelf |
op_relation |
https://dx.doi.org/10.1029/2019gl083881 https://dx.doi.org/10.1049/iet-rsn.2013.0053 https://dx.doi.org/10.1002/2014jf003246 https://dx.doi.org/10.3189/2015jog15j073 https://dx.doi.org/10.1126/science.1235798 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.96406510.1029/2019gl08388110.1049/iet-rsn.2013.005310.1002/2014jf00324610.3189/2015jog15j07310.1126/science.1235798 |
_version_ |
1795031642169933824 |